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El Nino's Surprising Steady Pacific Rains Can Affect World Weather
Scientists using data from a NASA satellite have found another piece in the global climate puzzle created by El Nino. El Nino events produce more of a steady rain in the middle of the Pacific Ocean. This is important because whenever there is a change in the amount and duration of rainfall over an area, such as the central Pacific, it affects weather regionally and even worldwide. The findings appeared in a paper authored by Courtney Schumacher and Robert Houze, atmospheric scientists at the University of Washington, Seattle, who used data from NASA's Tropical Rainfall Measuring Mission (TRMM) satellite to look at rainfall over the Pacific during the 1997-1998 El Nino. The study was published in a recent issue of the American Meteorological Society's Journal of Climate. El Nino occurs when warm water shifts from the western to the eastern Pacific Ocean and trade winds that usually blow from east to west across the equator diminish. As a result, rainfall patterns around the globe change during the life of these periodic climate events, and in some areas create floods or droughts. By identifying the changes in rainfall in one area of the globe, such as the central Pacific Ocean, scientists continue to piece together the El Nino puzzle that will help them improve rainfall forecasts around the world during the life of El Nino. Schumacher and Houze noticed an unusually steady rainfall over the central Pacific, much like a gray day with light rain and drizzle. That is surprising over the central Pacific, an area normally known for thunderstorms that build up during the heat of the day from rapidly rising air or convection, and then rain themselves out within an hour. "Instead, the rainfall we saw is called 'stratiform rain,' which are weaker rains that cover larger areas," Schumacher said. It's the type of rain that makes people want to stay inside all day. Seeing the difference between the convective and stratiform rain is very important to climatologists. Rain type matters because when water condenses and raindrops form, heat is released. That heat is a main driver in the circulation or movement of the atmosphere. "Convective rain, like from thunderstorms, releases heat lower in the atmosphere, while the steady, light, stratiform rain releases heat higher in the atmosphere," Houze said. Heat released at different levels of the atmosphere affects the vertical and horizontal movement of air. As a result, the heat from different types of rain can alter weather patterns, such as the familiar jet stream which impacts the United States. Weather prediction models benefit from better knowledge of the changing jet stream patterns, because storms like summer thunderstorms and winter snowstorms follow the path of the jet stream. The researchers noted that because increased stratiform rains warm the upper levels of the atmosphere, that additional heat strengthens the way air moves higher up and over a larger area than thunderstorm-generated rainfall. The larger area of air affected can impact weather patterns around the world. Although scientists are still uncertain why such large amounts of stratiform rain happen in the middle of the Pacific, especially during El Nino, observations from the TRMM satellite have allowed them to recognize this pattern. By identifying the type of rainfall, climatologists and meteorologists can make better rainfall forecasts in other areas of the world during the event. "That's the beauty of NASA's TRMM satellite," said Jeff Halverson, TRMM outreach scientist from NASA's Goddard Space Flight Center, Greenbelt, Md. "TRMM can see what's happening in remote areas of the tropics that can have affects on the rest of the world." Related Links TRMM AMS SpaceDaily Search SpaceDaily Subscribe To SpaceDaily Express 
El Nino's Soggy Secret
Washington - May 07, 2003Researchers have discovered how El Nino moves rainfall around the globe and are calling it El Nino's soggy secret. They did so by identifying rainfall patterns in the Pacific Ocean during the life of these periodic climate events, during which waters in the eastern Pacific Ocean warm up.
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